Trench-slope controlled deep-sea clastics in the exposed lower Surma Group in the southeastern fold belt of the Bengal Basin, Bangladesh

Author:

Gani M.Royhan,Alam M.Mustafa

Publisher

Elsevier BV

Subject

Stratigraphy,Geology

Reference46 articles.

1. Geology and depositional history of Cenozoic sediments of the Bengal Basin of Bangladesh;Alam;Palaeogeogr., Palaeoclimatol., Palaeoecol.,1989

2. Alam, M.M., 1995. Tide-dominated sedimentation in the Upper Tertiary succession of the Sitapahar anticline, Bangladesh. In: Flemming, B.W., Bortholoma, A. (Eds.), Tidal Signatures in Modern and Ancient Sediments. Int. Assoc. Sedimentol., Spec. Publ. 24, 329–341.

3. Alam, M., 1997. Bangladesh. In: Moores, E.M., Fairbridge, R.W. (Eds.), Encyclopedia of European and Asian Regional Geology. Chapman and Hall, London, pp. 64–72.

4. Lithofacies analysis and depositional environment of the Lichubagan Sandstone Formation (Upper Tertiary) in the Sitapahar anticline, south-eastern Folded Belt of Bangladesh;Alam;J. Indian Assoc. Sedimentol.,1995

5. Facies and environmental analysis of the Neogene (Surma Group) clastic succession in the Mirinja anticline, Folded Belt of the Bengal Basin, Bangladesh;Alam;Bangladesh Geosci. J.,1997

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